Treptichnus pedum (Seilacher, 1955)
Hammersburg et al., 2018
Diagnosis.—Treptichnus burrow system consisting of subhorizontal, straight to curved primary burrow with multiple successive burrow segments branching off in regular intervals (Fillion & Pickerill, 1990; Jensen, 1997).
Hofmann et al., 2012
Remarks.—Treptichnus is interpreted as a fodinichnion made by vermiform animals (Buatois et al., 1998). Recent neoichnologic work has convincingly argued for a priapulid origin for Treptichnus pedum (Vannier et al., 2010). Originally described as Phycodes pedum (Seilacher, 1955), Jensen (1997) referred this ichnospecies to Treptichnus whereas Geyer and Uchman (1995) placed it in Trichophycus. The type specimen (Seilacher, 1955, p. 387, fig. 4a) shows branching at the end of the burrow system resulting in a sickle-shaped appearance. Jensen (1997) included more irregular branching patterns with curved to highly winded courses and alternating or single sided segments. The proposal by Jensen (1997) became generally accepted (e.g., Seilacher et al., 2005; Seilacher, 2007; Vannier et al., 2010). Although the scarcity and incomplete nature of the Hanneh specimens prevent from a definite assignment, the overall morphology corresponds with descriptions by Jensen (1997).
Organism group | Biota |
Ichnofossil group | Ichnofossils |
Bioturbation trace fossils | |
Genus | Treptichnus |
Species | aequalternus |
apsorum | |
bifurcus | |
coronatum | |
lublinensis | |
meandrinus | |
pedum | |
pollardi | |
rectangularis | |
triplex | |
vagans |
- Palij et al., 1979 Jägala F-110 borehole 133.5 - 135 Lower Cambrian (old nomenclature)
- Palij et al., 1979 Koluvere 12 borehole 285.5 - 285.5 Lower Cambrian (old nomenclature)
- Toom et al., 2019a Rohuküla Quarry Raikküla Stage
- Jensen & Grant, 1998 Luovårri, Sweden Lower Cambrian (old nomenclature)
- Kowalski, 1987 Kurozweki outcrop Lower Cambrian (old nomenclature)